人文与经济地理学的传承与创新：青年学者的行动

2018年是中国改革开放40周年,也是“科学的春天”40周年。随着中国进入特色社会主义新时代,人文与经济地理学也将迈入新时代。青年学者恰好处在承前启后的这一时期,围绕学科传承和创新发展需要,面向新时代国家和经济社会发展的现实需求,青年学者积极行动起来,努力学习和传承人文与经济地理学前辈所建立的学科体系,并力图继续开拓和创新。一是助力建设学科文化,打造具有学科认同感和归属感的学术共同体。二是在向西方学习的同时,加强中国特色的自主理论建构与创新。三是向相关学科方向学习,加强交叉与综合的数据和方法创新,建设科学化、多元化的研究方法体系。四是青年学者更需要踏实认真的态度,找准个人研究领域方向,求真务实并力图创造新的知识,不断提升研究深度。人文与经济地理学的学科梦必将在一代代青年学者的接力奋斗中变为现实。     

Deformation, static recrystallization, and reactive melt transport in shallow subcontinental mantle xenoliths (Tok Cenozoic volcanic field, SE Siberia)

Partial melting and reactive melt transport may change the composition, microstructures, and physical properties of mantle rocks. Here we explore the relations between deformation and reactive melt transport through detailed microstructural analysis and crystallographic orientation measurements in spinel peridotite xenoliths that sample the shallow lithospheric mantle beneath the southeastern rim of the Siberian craton. These xenoliths have coarse-grained, annealed microstructures and show petrographic and chemical evidence for variable degrees of reaction with silicate melts and fluids, notably Fe-enrichment and crystallization of metasomatic clinopyroxene (cpx). Olivine crystal preferred orientations (CPO) range from strong to weak. [010]-fiber patterns, characterized by a point concentration of [010] normal to the foliation and by dispersion of [100] in the foliation plane with a weak maximum parallel to the lineation, predominate relative to the [100]-fiber patterns usually observed in lithospheric mantle xenoliths and peridotite massifs. Variations in olivine CPO patterns or intensity are not correlated with modal and chemical compositions. This, together with the analysis of microstructures, suggests that reactive melt percolation postdated both deformation and static recrystallization. Preferential crystallization of metasomatic cpx along (010) olivine grain boundaries points to an influence of the preexisting deformation fabrics on melt transport, with higher permeability along the foliation. Similarity between orthopyroxene (opx) and cpx CPO suggests that cpx orientations may be inherited from those of opx during melt-rock reaction. As observed in previous studies, reactive melt transport does not weaken olivine CPO and seismic anisotropy in the upper mantle, except in melt accumulation domains. In contrast, recovery and selective grain growth during static recrystallization may lead to development of [010]-fiber olivine CPO and, if foliations are horizontal, result in apparent isotropy for vertically propagating SKS waves, but strong anisotropy for horizontally propagating surface waves.     

中国金矿床成矿时代初探

本文以夹皮沟、辽宁、冀东、张家口、小秦岭、胶东、湘西、粤西-海南、三江、北疆和台湾等重要金矿比集中区为例,讨论了我国不同地区某些典型金矿床的成矿年龄,并在此基础上概括了我国不同地质时期金矿床的分布特征、矿床类型和成矿环境。在金矿成矿历史上存在一老（晚太古代-早元古代）一新（中新生代）两个成矿高峰时期,前者以形成绿岩建造金矿床为特征,后者则以发育花岗岩建造金矿床为特征。"成矿物质来源年龄老,矿床定位年龄新",即成矿作用具有明显继承性是中国金矿床最突出的特征。     

世界遗产地旅游产品开发的创新思考

遗产旅游已经成为人们最火爆的旅游产品。然而,世界遗产地旅游产品开发值得我们深思。对世界遗产地旅游产品开发的要求、世界遗产地旅游产品应该具有的特征、世界遗产地适宜开发的旅游产品类型、旅游产品开发模式等方面进行了重新思考,利于世界遗产的保护。     

关于长白山申报世界遗产可行性分析

本文根据《保护世界文化及自然遗产公约》和《执行世界遗产公约的操作准则》的要求，详细的论述了长白山的基本情况、科学价值、文化价值、美学价值等内容，认为长白山符合定义、达到准则的要求以及“整体环境”的条件要求。有关部门应该积极组织长白山申报世界遗产的工作，提高国际知名度，受到国际社会的保护，真正使长白山的保护达到世界标准。     

新时期中华民族精神的培育

民族精神是一个民族赖以生存和发展的精神支撑。建设中国特色的社会主义现代化事业是一项前无古人的伟大创举 ,它更加需要一种积极向上的民族精神的支撑。培育新时期的中华民族精神是我们的一项重要任务 ,在培育民族精神的时候应该继承民族文化的优秀传统 ,吸收其他民族文化的优秀成分 ,同时又要使民族精神保持与时俱进 ,不断丰富和发展     

四川盆地东缘寒武系盐下油气勘探领域探讨

地球物理资料显示四川盆地东缘齐岳山附近寒武系高台组膏盐岩层下深部存在逆冲构造,其形成过程以及油气地质意义未见深入研究。笔者等综合四川盆地东部石柱地区线束三维和建南地区二维地震反射资料,并结合钻井资料以及区域地质研究成果,从构造继承性的角度探讨四川盆地震旦系灯影组台缘带类型,并分析了川东地区寒武系盐下油气圈闭特征。研究获得如下认识：① 川东齐岳山北段构造变形强烈,普遍发育基底卷入构造,构造样式受青白口纪—南华纪裂谷与转换带构造位置的控制。② 依据构造继承关系将盆内灯影组台缘带划分为德阳—安岳地区原生型台缘带、万源—达州地区继承型台缘带以及石柱地区继承—改造型台缘带。③ 依据青白口纪—南华纪裂谷的分布和后期构造作用影响大小,认为沿齐岳山向南至南川一带存在与石柱地区相似的灯影组继承—改造型台缘带,忠县、南川以西存在灯影组继承型台缘带。④ 研究区新元古界—下寒武统烃源岩、灯影组—龙王庙组滩相白云岩储层与寒武系膏盐岩层系构成完整的生储盖组合。⑤ 寒武系盐下基底逆冲可形成成排、成带的构造,与灯影组继承—改造型台缘带、龙王庙组滩相白云岩储层配置,形成断层相关的构造—岩性圈闭带,成为川东地区油气规模聚集有利区。研究认为四川盆地东部石柱地区震旦纪—早寒武世早期继承了青白口纪—南华纪裂谷构造特征,燕山期构造反转,高台组盐下形成基底卷入逆冲构造,具备生储盖等基本石油地质条件,具有重要的油气勘探现实意义。     

Multistage tectono-stratigraphic evolution of the Canavese Intracontinental Suture Zone: New constraints on the tectonics of the Inner Western Alps

The Canavese Intracontinental Suture Zone (CISZ) within the Inner Western Alps represents the remnant of a long-lived minor subduction zone involving a narrow, thinned continental crust/oceanic lithosphere seaway between two continental domains of the Adria microplate (i.e., the Sesia Zone and the Ivrea-Verbano Zone). As opposed to many suture zones, the CISZ mostly escaped pervasive tectonic deformation and metamorphism, thus preserving the original stratigraphy and allowing the relationships between tectonics and sedimentation to be defined. Through detailed geological mapping (1:5000 scale), structural analysis, stratigraphic and petrographic observations, we document evidences for the late Paleozoic to late Cenozoic tectonic evolution of the CISZ, showing that it played a significant role in the context of the tectonic evolution of the Inner Western Alps region from the early to late Permian Pangea segmentation, to the Jurassic Tethyan rifting, and up to the subduction and collisional stages, forming the Western Alps. The site of localization/formation of the CISZ was not accidental but associated with the re-use of structures inherited from regional-scale wrench tectonics related to the segmentation of Pangea, and from the subsequent extensional tectonics related to the Mesozoic rifting, as documented by crosscutting relationships between stratigraphic unconformities and tectonic features. Our findings document that evidences derived from stratigraphy, facies indicators, and relationships between tectonics and sedimentation in the shallow crustal portions of suture zones, such in the CISZ, are important to better constrain the tectonic history of those metamorphic orogenic belts around the world in which evolutionary details are commonly complicated by high-strain deformation and metamorphic transformations.     

Inheritance mode of microsatellite loci and their use for kinship analysis in the Pacific oyster （Crassostrea gigas）

Five full-sib families of the Pacific oyster(Crassostrea gigas) larvae were used to study the mode of inheritance at eight microsatellite loci,and the feasibility of these markers for kinship estimate was also examined.All eight microsatellite loci were compatible with Mendelian inheritance.Neither evidence of sex-linked barriers to transmission nor evidence of major barriers to fertilization between gametes from the parents was shown.Three of the eight loci showed the presence of null alleles in four families,demonstrating the need to conduct comprehensive species-specific inheritance studies for microsatellite loci used in population genetic studies.Although the null allele heterozygotes were considered as homozygotes in the calculation of genetic distance,offspring from five full-sib families were unambiguously discriminated in the neighbor-joining dendrogram.This result indicates that the microsatellite markers may be capable of discriminating between related and unrelated oyster larvae in the absence of pedigree information,and is applicable to the investigation of the effective number of parents contributing to the hatchery population of the Pacific oyster.     

Inheritance mode of microsatellite loci and their use for kinship analysis in the Pacific oyster （Crassostrea gigas）

Five full-sib families of the Pacific oyster （Crassostrea gigas） larvae were used to study the mode of inheritance at eight microsatellite loci, and the feasibility of these markers for kinship estimate was also examined. All eight microsatellite loci were compatible with Mendelian inheritance. Neither evidence of sex-linked barriers to transmission nor evidence of major barriers to fertilization between gametes from the parents was shown. Three of the eight loci showed the presence of null alleles in four families, demonstrating the need to conduct comprehensive species-specific inheritance studies for microsatellite loci used in population genetic studies. Although the null allele heterozygotes were considered as homozygotes in the calculation of genetic distance, offspring from five full-sib families were unambiguously discriminated in the neighbor-joining dendrogram. This result indicates that the microsatellite markers may be capable of discriminating between related and unrelated oyster larvae in the absence of pedigree information, and is applicable to the investigation of the effective number of parents contributing to the hatchery population of the Pacific oyster.